» Articles » PMID: 35770981

As a Major Consumer of Fixed Nitrogen

Overview
Specialty Microbiology
Date 2022 Jun 30
PMID 35770981
Authors
Affiliations
Soon will be listed here.
Abstract

Crocosphaera watsonii (hereafter referred to as ) is a key nitrogen (N) fixer in the ocean, but its ability to consume combined-N sources is still unclear. Using microcosm incubations with an ecological model, we show that has high competitive capability both under low and moderately high combined-N concentrations. In field incubations, accounted for the highest consumption of ammonium and nitrate, followed by picoeukaryotes. The model analysis shows that cells have a high ammonium uptake rate (~7 mol N [mol N] d at the maximum), which allows them to compete against picoeukaryotes and nondiazotrophic cyanobacteria when combined N is sufficiently available. Even when combined N is depleted, their capability of nitrogen fixation allows higher growth rates compared to potential competitors. These results suggest the high fitness of in combined-N limiting, oligotrophic oceans heightening its potential significance in its ecosystem and in biogeochemical cycling. Crocosphaera watsonii is as a key nitrogen (N) supplier in marine ecosystems, and it has been estimated to contribute up to half of oceanic N fixation. Conversely, a recent study reported that can assimilate combined N and proposed that unicellular diazotrophs can be competitors with non-N fixing phytoplankton for combined N. Despite its importance in nitrogen cycling, the methods by which compete are not currently fully understood. Here, we present a new role of as a combined-N consumer: a competitor against nondiazotrophic phytoplankton for combined N. In this study, we combined microcosm experiments and an ecosystem model to quantitatively evaluate the combined-N consumption by and other non-N fixing phytoplankton. Our results suggest the high fitness of in combined-N limiting, oligotrophic oceans and, thus, heightens its potential significance in its ecosystem and in biogeochemical cycling.

Citing Articles

Eddy-driven diazotroph distribution in the subtropical North Atlantic: horizontal variability prevails over particle sinking speed.

Cerdan-Garcia E, Alvarez-Salgado X, Aristegui J, Martinez-Marrero A, Benavides M Commun Biol. 2024; 7(1):929.

PMID: 39095605 PMC: 11297262. DOI: 10.1038/s42003-024-06576-w.


Coexistence of Dominant Marine Phytoplankton Sustained by Nutrient Specialization.

Masuda T, Inomura K, Mares J, Kodama T, Shiozaki T, Matsui T Microbiol Spectr. 2023; 11(4):e0400022.

PMID: 37458590 PMC: 10441275. DOI: 10.1128/spectrum.04000-22.

References
1.
Thompson A, Foster R, Krupke A, Carter B, Musat N, Vaulot D . Unicellular cyanobacterium symbiotic with a single-celled eukaryotic alga. Science. 2012; 337(6101):1546-50. DOI: 10.1126/science.1222700. View

2.
Montoya J, Voss M, Kahler P, Capone D . A Simple, High-Precision, High-Sensitivity Tracer Assay for N(inf2) Fixation. Appl Environ Microbiol. 1996; 62(3):986-93. PMC: 1388808. DOI: 10.1128/aem.62.3.986-993.1996. View

3.
Sargent E, Hitchcock A, Johansson S, Langlois R, Moore C, Laroche J . Evidence for polyploidy in the globally important diazotroph Trichodesmium. FEMS Microbiol Lett. 2016; 363(21). DOI: 10.1093/femsle/fnw244. View

4.
Morozov A . Emergence of Holling type III zooplankton functional response: bringing together field evidence and mathematical modelling. J Theor Biol. 2010; 265(1):45-54. DOI: 10.1016/j.jtbi.2010.04.016. View

5.
Ackleson S, Spinrad R . Size and refractive index of individual marine participates: a flow cytometric approach. Appl Opt. 2010; 27(7):1270-7. DOI: 10.1364/AO.27.001270. View